Recoverable Creep Deformation and Transient Local Stress Concentration Due to Heterogeneous Grain-Boundary Diffusion and Sliding in Polycrystalline Solids

Total Page:16

File Type:pdf, Size:1020Kb

Recoverable Creep Deformation and Transient Local Stress Concentration Due to Heterogeneous Grain-Boundary Diffusion and Sliding in Polycrystalline Solids ARTICLE IN PRESS Journal of the Mechanics and Physics of Solids 56 (2008) 1460–1483 www.elsevier.com/locate/jmps Recoverable creep deformation and transient local stress concentration due to heterogeneous grain-boundary diffusion and sliding in polycrystalline solids Yujie Wei, Allan F. BowerÃ, Huajian GaoÃÃ Division of Engineering, Brown University, Box D, Providence, RI 02912, USA Received 8 June 2007; received in revised form 14 August 2007; accepted 15 August 2007 Abstract Numerical simulations are used to investigate the influence of heterogeneity in grain-boundary diffusivity and sliding resistance on the creep response of a polycrystal. We model a polycrystal as a two-dimensional assembly of elastic grains, separated by sharp grain boundaries. The crystal deforms plastically by stress driven mass transport along the grain boundaries, together with grain-boundary sliding. Heterogeneity is idealized by assigning each grain boundary one of two possible values of diffusivity and sliding viscosity. We compute steady state and transient creep rates as functions of the diffusivity mismatch and relative fractions of grain boundaries with fast and slow diffusion. In addition, our results show that under transient conditions, flux divergences develop at the intersection between grain boundaries with fast and slow diffusivity, which generate high local stress concentrations. The stress concentrations develop at a rate determined by the fast diffusion coefficient, and subsequently relax at a rate determined by the slow diffusion coefficient. The influence of the mismatch in diffusion coefficient, loading conditions, and material properties on the magnitude of this stress concentration is investigated in detail using a simple model problem with a planar grain boundary. The strain energy associated with these stress concentrations also makes a small fraction of the plastic strain due to diffusion and sliding recoverable on unloading. We discuss the implications of these results for conventional polycrystalline solids at high temperatures and for nanostructured materials where grain-boundary diffusion becomes one of the primary inelastic deformation mechanisms even at room temperature. r 2007 Published by Elsevier Ltd. Keywords: Recoverable creep deformation; Grain-boundary diffusion; Grain-boundary sliding; Transient stress concentration 1. Introduction Grain-boundary (GB) diffusion and sliding are the dominant mechanisms of plastic deformation in polycrystalline metals and ceramics at high homologous temperatures. They also contribute to room- temperature plastic flow in nanocrystalline materials, where the fine grain size tends to suppress plastic flow by ÃCorresponding author. ÃÃAlso corresponding author. E-mail addresses: [email protected] (A.F. Bower), [email protected] (H. Gao). 0022-5096/$ - see front matter r 2007 Published by Elsevier Ltd. doi:10.1016/j.jmps.2007.08.007 ARTICLE IN PRESS Y. Wei et al. / J. Mech. Phys. Solids 56 (2008) 1460–1483 1461 dislocation motion while the high density of GBs accelerates diffusional creep. In addition, GB diffusion plays an important role in stress generation and relaxation in polycrystalline thin films. GB diffusional creep in macroscopic polycrystals has been extensively studied. Nabarro (1948) and Herring (1950) first pointed out that self-diffusion can cause crystals to change shapes and induce macroscopic plastic deformation at elevated temperatures. Coble (1963) studied the dependence of macroscopic strain rates _ on grain size l and applied tensile stress s due to collective GB diffusion and showed that dDO s _ ¼ a 3 , (1) kBT l where a is a geometrical constant, D is the GB diffusivity and d is the thickness of a layer in which interface diffusion is supposed to take place; kB, T and O are the Boltzman constant, the absolute temperature and the atomic volume, respectively. Ashby and Verrall (1973) considered a geometrical model of creep flow taking into account strains due to GB diffusion and sliding, to reflect the fact that both GB diffusion and sliding plays an increasingly important role in the inelastic deformation of polycrystalline solids as the temperature rises or the grain size decreases. More recent work has extended the original Coble model by accounting for phenomena such as interface reactions (Ashby, 1969, 1972; Arzt et al., 1983; Cocks, 1992). In general, these models predict a nonlinear relationship between stress and strain rate. Numerical methods have been developed to study GB diffusion and associated mechanical behavior in polycrystalline solids. Needleman and Rice (1980) have first applied the finite-element method in modeling GB diffusion and creep. Pan and Cocks (1993) developed finite-element formulations for modeling GB diffusion in arbitrary networks of grains with straight GBs. They applied the numerical techniques, combined with a time integration algorithm, to study microstructure evolution during superplastic deformation in polycrystalline materials. Bower and Wininger (2004) extended the work of Pan and Cocks (1993) by using an advancing front algorithm to generate a sequence of adaptive, evolving finite-element meshes to solve the evolution of two-dimensional geometries. Sethian and Wilkening (2003) and Wilkening et al. (2004a,b) have used techniques from semigroup theory to study mass transport in microelectronic circuits due to electromigration and GB diffusion. GB diffusion is also an important stress relaxation mechanism in thin films based on experimental observations (Thouless et al., 1996; Kobrinsky and Thompson, 1998) and theories (Gao et al., 1999; Weiss et al., 2001; Guduru et al., 2003). Meanwhile, it has been observed to act in combination with other deformation mechanisms in thin films. For example, recent studies on the mechanical behaviors of polycrystalline thin films on substrates (Gao et al., 1999) have indicated that constrained GB diffusion1 induces crack-like singular stress fields which leads to novel dislocation mechanisms that are driven by locally induced, rather than globally applied, stresses. In situ TEM experiments (Balk et al., 2003), atomistic simulations (Buehler et al., 2003) and discrete dislocation simulations (Hartmaier et al., 2005) have shown that such constrained GB diffusion and the associated dislocation mechanisms dominate plastic deformation mechanisms in unpassivated films thinner than a few hundred nanometers. These studies are calling for broader investigations on the general importance of constrained GB diffusion mechanisms in polycrystalline materials. Coble-type GB diffusional creep, together with GB sliding accommodated by GB diffusion, have been considered as major deformation mechanisms in nanocrystalline materials by many authors (e.g., Gleiter, 1989). Although diffusion-controlled processes are typically activated only at high homologous temperatures, Yamakov et al. (2002) have argued, based on their molecular dynamics simulations, that Coble-creep should be a dominating mechanism in nanocrystalline materials even at low homologous temperatures. An important feature of plastic deformation controlled by GB diffusion is that it gives rise to a strain-rate sensitivity on the order of 1. Although strain-rate sensitivity around 1 is rarely observed in regular tensile and compressive tests for nanocrystalline materials, significantly enhanced strain-rate sensitivity has been reported in both h.c.p. and f.c.c. nc materials. Nc Cu synthesized by Jiang et al. (2006) showed a rate sensitivity about m ¼ 0:104 at room 1In columnar grain structures in thin films on substrates, diffusion tends to generate stress singularities at the ends of GBs that terminate perpendicular to the substrate, if diffusion between thin films and substrates are constrained. These stress singularities may lead to dislocation emission and initiate delamination. GB diffusion in such a situation is termed as ‘constrained GB diffusion’. ARTICLE IN PRESS 1462 Y. Wei et al. / J. Mech. Phys. Solids 56 (2008) 1460–1483 1000 4 × 10-1/s 800 4 × 10-2/s 4 × 10-3/s 600 4 × 10-4/s 4 × 10-5/s Stress (MPa) 400 4 × 10-6/s 200 2 × 10-6/s 10-6/s 0 0 2 4 6 Strain (%) Fig. 1. Stress–strain curves of brush-plated nanocrystalline Cu at different strain rates. Data replotted from Jiang et al. (2006). temperature in the strain rate range of 10À6=sto4Â 10À1=s, Fig. 1. The authors have attributed the high strain-rate sensitivity to the dominant unstructured high-angle GBs in the material. With the current technological trends in continuing miniaturization of structures in electronic devices and materials, a thorough understanding of the inelastic deformation mechanisms by GB diffusion and GB sliding is becoming increasingly important. On the other hand, existing experiments and theories have not been able to fully capture the complex interplay between different deformation mechanisms in GBs. In particular, the following issues are of interest for the present study. Most existing theories have assumed homogeneous diffusivity in GBs. In reality, most material properties are heterogeneous at the scale of individual grains; high angle, relatively unstructured GBs usually have higher diffusivities compared to low angle, structured GBs. GB diffusivity in a polycrystalline solid could differ by several orders of magnitude from one grain to another. Constrained GB diffusion due to heterogeneous diffusivities can affect not only deformation mechanisms in GBs, but also those in grain interiors. Diffusional deformation in GBs is a kinetic process but existing theories are
Recommended publications
  • The Viscosities of Partially Molten Materials Undergoing Diffusion Creep
    The viscosities of partially molten materials undergoing diffusion creep John F. Rudge Bullard Laboratories, Department of Earth Sciences, University of Cambridge December 10, 2018 Abstract Partially molten materials resist shearing and compaction. This resistance is described by a fourth-rank effective viscosity tensor. When the tensor is isotropic, two scalars determine the resistance: an effective shear and an effective bulk viscosity. Here, calculations are presented of the effective viscosity tensor during diffusion creep for a 2D tiling of hexagonal unit cells and a 3D tessellation of tetrakaidecahedrons (truncated octahedrons). The geometry of the melt is determined by assuming textural equilibrium. The viscosity tensor for the 2D tiling is isotropic, but that for the 3D tessellation is anisotropic. Two parameters control the effect of melt on the viscosity tensor: the porosity and the dihedral angle. Calculations for both Nabarro-Herring (volume diffusion) and Coble (surface diffusion) creep are presented. For Nabarro-Herring creep the bulk viscosity becomes singular as the porosity vanishes. This singularity is logarithmic, a weaker singularity than typically assumed in geodynamic models. The presence of a small amount of melt (0.1% porosity) causes the effective shear viscosity to approximately halve. For Coble creep, previous modelling work has argued that a very small amount of melt may lead to a substantial, factor of 5, drop in the shear viscosity. Here, a much smaller, factor of 1.4, drop is obtained for tetrakaidecahedrons. Owing to a Cauchy relation symmetry, the Coble creep bulk viscosity is a constant multiple of the shear viscosity when melt is present. 1 Introduction Dynamical models are often highly dependent on assumptions about the rheology of the material being deformed.
    [Show full text]
  • The Role of Pressure Solution Creep in the Ductility of the Earth's
    The role of pressure solution creep in the ductility of the earth’s upper crust Jean-Pierre Gratier, Dag Dysthe, Francois Renard To cite this version: Jean-Pierre Gratier, Dag Dysthe, Francois Renard. The role of pressure solution creep in the ductility of the earth’s upper crust. Advances in Geophysics, Elsevier, 2013, 54, pp.47-179. 10.1016/B978-0- 12-380940-7.00002-0. insu-00799131 HAL Id: insu-00799131 https://hal-insu.archives-ouvertes.fr/insu-00799131 Submitted on 11 Mar 2013 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. 1 The role of pressure solution creep in the ductility of the Earth’s upper crust Jean-Pierre Gratier1, Dag K. Dysthe2,3, and François Renard1,2 1Institut des Sciences de la Terre, Observatoire, CNRS, Université Joseph Fourier-Grenoble I, BP 53, 38041 Grenoble, France 2Physics of Geological Processes, University of Oslo, Norway 3Laboratoire Interdisciplinaire de Physique, BP 87, 38041 Grenoble, France The aim of this review is to characterize the role of pressure solution creep in the ductility of the Earth’s upper crust and to describe how this creep mechanism competes and interacts with other deformation mechanisms.
    [Show full text]
  • Grain-Sizereductionmechanisms and Rheologicalconsequences in High
    Grain-sizereductionmechanisms and rheologicalconsequences in high-temperaturegabbromylonites of Hidaka, Japan Hugues Raimbourg, Tsuyoshi Toyoshima, Yuta Harima, Gaku Kimura To cite this version: Hugues Raimbourg, Tsuyoshi Toyoshima, Yuta Harima, Gaku Kimura. Grain- sizereductionmechanisms and rheologicalconsequences in high-temperaturegabbromylonites of Hidaka, Japan. Earth and Planetary Science Letters, Elsevier, 2008, 267 (3-4), pp.637-653. 10.1016/j.epsl.2007.12.012. insu-00756068 HAL Id: insu-00756068 https://hal-insu.archives-ouvertes.fr/insu-00756068 Submitted on 22 Nov 2012 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Grain size reduction mechanisms and rheological consequences in high-temperature gabbro mylonites of Hidaka, Japan Hugues Raimbourga, Tsuyoshi Toyoshimab, Yuta Harimab, Gaku Kimuraa (a) Department of Earth and Planetary Science, Faculty of Science, University of Tokyo, Japan (b) Department of Geology, Faculty of Science, University of Niigata, Japan Corresponding Author: Hugues Raimbourg, Dpt. Earth Planet. Science, Faculty
    [Show full text]
  • Dislocation and Diffusion Creep of Synthetic Anorthite Aggregates
    JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 105, NO. Bll, PAGES 26,017-26,036, NOVEMBER 10, 2000 Dislocation and diffusion creep of synthetic anorthite aggregates E. Rybacki and G. Dresen GeoForschungsZentrumPotsdam, Potsdam, Germany Abstract. Syntheticfine-grained anorthite aggregates were deformedat 300 MPa confining pressurein a Paterson-typegas deformation apparatus. Creep tests were performedat temperatures rangingfrom 1140 to 1480K, stressesfrom 30 to 600 MPa, and strain rates between 2x 10 '6 and lx10-3 s 'l. Weprepared samples with water total contents of 0.004 wt % (dry)and 0.07 wt % (wet), respectively.The wet (dry) materialcontained <0.7 (0.2) vol % glass,associated with fluid inclusionsor containedat triplejunctions. The arithmeticmean grain size of the specimensvaried between2.7 _+0.1 lamfor the dry materialand 3.4 _+0.2 lamfor wet samples.Two differentcreep regimeswere identified for dry andwet anorthiteaggregates. The datacould be fitted to a power law. At stresses> 120 MPa we founda stressexponent of n = 3 irrespectiveof the water content, indicatingdislocation creep. However, the activation energy of wetsamples is356 _+ 9 kJmol 'l, substantiallylower than for dry specimens with 648 + 20kJ mo1-1. The preexponential factor is log A = 2.6(12.7) MPa -n s -• forwet (dry) samples. Microstructural observations suggest that grain boundarymigration recrystallization is importantin accommodatingdislocation creep. In the low- stressregime we observeda stressexponent of n = 1, suggestingdiffusion creep. The activation energiesfor dry and wet samples are 467 + 16and 170 + 6 kJmol '•, respectively.Log A is 12.1 MPa-n pm m s -1 for the dry material and 1.7 MPa -" pm m s '1 for wet anorthite.
    [Show full text]
  • Grainsize Sensitive Rheology of Orthopyroxene
    PUBLICATIONS Geophysical Research Letters RESEARCH LETTER Grain-size sensitive rheology of orthopyroxene 10.1002/2014GL060607 Rolf H.C. Bruijn1 and Philip Skemer1 Key Points: 1Department of Earth and Planetary Sciences, Washington University in St. Louis, Saint Louis, Missouri, USA • Deformation mechanism map for orthopyroxene is constructed • Diffusion creep of orthopyroxene is important over a wide range Abstract The grain-size sensitive rheology of orthopyroxene is investigated using data from rheological of conditions and microstructural studies. A deformation mechanism map is constructed assuming that orthopyroxene deforms by two independent mechanisms: dislocation creep and diffusion creep. The field boundary between these mechanisms is defined using two approaches. First, experimental data from Lawlis (1998), Correspondence to: which show a deviation from non-linear power law behavior at low stresses, are used to prescribe the location R. H. C. Bruijn, of the field boundary. Second, a new orthopyroxene grain-size piezometer is used as a microstructural [email protected] constraint to the field boundary. At constant temperature, both approaches yield sub-parallel field boundaries, separated in grain size by a factor of only 2–5. Extrapolating to lithospheric conditions, the Citation: deformation mechanism transition occurs at a grain size of ~150–500 μm, consistent with observations from Bruijn, R. H. C., and P. Skemer (2014), nature. As the transition from dislocation to diffusion creep may promote shear localization, grain-size Grain-size sensitive rheology of orthopyroxene, Geophys. Res. Lett., 41, reduction of orthopyroxene may play a prominent role in plate-boundary deformation. doi:10.1002/2014GL060607. Received 20 MAY 2014 Accepted 3 JUL 2014 1.
    [Show full text]
  • Dislocations and Dislocation Creep
    Dislocations and dislocation creep... 1. Introduction: a) Observations of textures associated with dislocation creep b) MOVIES of dislocations in metals. 2. How do dislocations move?: single dislocations: stress, energy and motion. Orowan’s equation. Frank-Read sources, Work Hardening (Fatigue, paper clips) 3. Recovery: dislocation climb, subgrain formation 4. Recrystallization: Fabric development and grain size evolution Grain rotation (LPO development) Reduction: Mechanisms of recrystallization Growth: forces driving grain growth... ----> Localization REVISIT THE QUARTZ regimes 5. Grain Growth: static and dynamic ? Thursday: 6. Piezometers and Wattmeters Empirical Piezometers (dislocations, subgrain and grain size). Stress in the lithosphere from xenoliths (Mercier) Stress across shear zones (Kohlstedt and Weathers) The WATTMETER 1. Intro: Observations First, ALL the complexity that we want to understand ! THEN, deconstruction: simple - - - - > complex small scale (single dislocation) ----- > larger scale (behavior of ensembles) Journal of Structural Geology, Vol. 14, No. 2, pp. 145 to 159, 1992 0191-8141/92 $05.00+0.00 Printed in Great Britain (~ 1992 Pergamon Press plc Dislocation creep regimes in quartz aggregates Journal of Structural Geology, Vol. 14, No. 2, pp. 145 to 159, 1992 Dislocation creep regimes in quartz aggregate0s 191-8141/92 $05.00+0.00 147 Printed in Great GBritainREG HIRrH and JAN TULLIS (~ 1992 Pergamon Press plc 1400 Departmreengimest of Geolo gdetericalS cieminednces, Brow bn Uyn relativiversity,P reo vidence, RI 02912, U.S.A. rates of (Received 11 September 1990; accepted in revised form 30 June 1991) 1. dislocation productionDislocation creep regimes in quartz aggregates Abstract--Using opti2.ca l dislocationand TEM microsc oclimbpy we have determined that threei regimes of dislocation creep ocRcur.
    [Show full text]
  • Formation of Lithospheric Shear Zones
    Physics of the Earth and Planetary Interiors 270 (2017) 195–212 Contents lists available at ScienceDirect Physics of the Earth and Planetary Interiors journal homepage: www.elsevier.com/locate/pepi Formation of lithospheric shear zones: Effect of temperature on two-phase grain damage ⇑ Elvira Mulyukova a, , David Bercovici a a Yale University, Department of Geology and Geophysics, New Haven, CT, USA article info abstract Article history: Shear localization in the lithosphere is a characteristic feature of plate tectonic boundaries, and is evident Received 17 February 2017 in the presence of small grain mylonites. Localization and mylonitization in the ductile portion of the Received in revised form 15 June 2017 lithosphere can arise when its polymineralic material deforms by a grain-size sensitive rheology in com- Accepted 24 July 2017 bination with Zener pinning, which can impede, or possibly even reverse, grain growth and thus pro- Available online 1 August 2017 motes a self-softening feedback mechanism. However, the efficacy of this mechanism is not ubiquitous and depends on lithospheric conditions such as temperature and stress. Therefore, we explore the con- Keywords: ditions under which self-weakening takes place, and, in particular, the effect of temperature and defor- Shear zones mation state (stress or strain-rate) on these conditions. In our model, the lithosphere-like polymineralic Grain damage mechanics Mylonites material is deformed in a two-dimensional simple shear driven by constant stress or strain rate. The min- eral grains evolve to a stable size, which is obtained when the rate of coarsening by normal grain growth and the rate of grain size reduction by damage are in balance.
    [Show full text]
  • Diffusion Creep
    Diffusion Creep Poirier, Chapter 2 and 7, 1985. Gordon, 1985. Monday, Nov. 3, 2003 12.524 Mechanical properties of rocks Fick’s First Law: Driving Force ∇c z Chemical Diffusion ∇T z Thermal diffusion JD=−i ∇µ ∇V z Electrical conduction σ z Diffusion creep 12.524 Mechanical properties of rocks Types of Diffusion Mechanism Path Process Isotope Lattice Interdiffusion Self-diffusion Pipe Creep Vacancy Grain Boundary Ambipolar Interstitial Surface Ring Pore fluid 12.524 Mechanical properties of rocks Diffusion mechanisms Vacancy Diffusion Interstitial Ring Diffusion Collinear Direct Exchange Non -collinear Cyclic Exchange A B 12.524 Mechanical properties of rocks Vacancy–Assisted Diffusion From Site by Glicksman and Lupulescu, RPI, 2003 The FCC lattice geometry requires W = ( 3−1)Da = 0.73Da Images removed due to copyright considerations. For more information, see http://www.rpi.edu/~glickm/diffusion/ 12.524 Mechanical properties of rocks plan view Kinetics Equation for Vacancy Diffusion z Coefficient of Diffusivity for Self-diffusion not the same as Coefficient for Vacancy Diffusion DNDsd= vi v migration =−Nvoexp (∆∆ G vf / kT )i D v o exp − ( G vm / kT ) =−+DGGkTsd oexp (∆∆ vf vm )/ 12.524 Mechanical properties of rocks Diffusion Creep in Monatomic Solid z Basic Ideas Vacancies Supersaturated z Supersaturation of vacancies owing to stress z Diffusion results z Work done on mat’l Vacancies UndersaturatedVacancies by tractions z Energy dissipated in heat, entropy, and surface area 12.524 Mechanical properties of rocks Diffusion Creep z z Nabarro-Herring Creep Monatomic Lattice z Quasi static z Coble Creep z Vacancy Grain Boundary z Increasing length; Poisoining 12.524 Mechanical properties of rocks Critical Idea: Tension makes vacancy formation easier.
    [Show full text]
  • 8. TIME DEPENDENT BEHAVIOUR: CREEP in General, the Mechanical
    8. TIME DEPENDENT BEHAVIOUR: CREEP In general, the mechanical properties and performance of materials change with increasing temperatures. Some properties and performance, such as elastic modulus and strength decrease with increasing temperature. Others, such as ductility, increase with increasing temperature. It is important to note that atomic mobility is related to diffusion which can be described using Ficks Law: æ Q ö D = D exp - (8.1) O è RT ø where D is the diffusion rate, Do is a constant, Q is the activation energy for atomic motion, R is the universal gas constant (8.314J/mole K) and T is the absolute temperature. Thus, diffusion-controlled mechanisms will have significant effect on high temperature mechanical properties and performances. For example, dislocation climb, concentration of vacancies, new slip systems, and grain boundary sliding all are diffusion-controlled and will affect the behaviour of materials at high temperatures. In addition, corrosion or oxidation mechanisms, which are diffusion-rate dependent, will have an effect on the life time of materials at high temperatures. Creep is a performance-based behaviour since it is not an intrinsic materials response. Furthermore, creepis highly dependent on environment including temperature and ambient conditions. Creep can be defined as time-dependent deformation at absolute temperatures greater than one half the absolute melting. This relative T (abs ) temperature ( ) is know as the homologous temperate. Creep is a relative Tmp (abs ) phenomenon which may occur at temperatures not normally considered "high." Several examples illustrate this point. a) Ice melts at 0°C=273 K and is known to creep at -50°C=223 K.
    [Show full text]
  • Evaluation of Diffusion Creep in Low Melting Point Materials By
    397 Evaluation of Diffusion Creep in Low Melting Point Materials by Nanoindentation Creep Test∗ Tadahiro SHIBUTANI∗∗,QiangYU∗∗ and Masaki SHIRATORI∗∗ In this study, diffusion creep in Sn-37Pb as a low melting point alloy during a nanoin- dentation creep test was examined. The creep exponent, n, from the relationship between hardness and indenter dwell time decreases as a function of time and is saturated when n = 1. From observations of the indented surface, plastic deformation due to the indenter takes place in the early stages. On the other hand, granular deformation takes place in the middle and last stages. Finite element analysis revealed that the reduction in Mises stress is faster than that of hydrostatic stress. Multiaxial stresses appear below the indenter, and axial compo- nents of stress remain after relaxation. Since the core hydrostatic stress causes a gradient in the chemical potential at grain boundaries, diffusion creep affects the behavior of indentation creep in the last stage. A transition from power-law creep to diffusion creep occurs below the indenter. Key Words: Creep, Hardness, Finite Element Method, Nanoindentation, Diffusion Creep, and Low Temperature Melting Point Alloy area(7) – (12). Displacements into the surface are measured 1. Introduction continuously under a constant load, and the creep prop- At elevated temperatures, the mechanism of creep de- erties are extracted from the evolution of the hardness on formation in metals is classified into dislocation creep and the basis of the power-law creep relationship. Indenta- diffusion creep(1). Generally, dislocation creep (power- tion creep tests are widely employed as an approximate law creep) is dominant at higher stresses and elevated tem- method, and the creep properties obtained from inden- peratures.
    [Show full text]
  • Research Creep Deformation and Fracture Processes in of and OFF
    SKI Report 2005:18 Research Creep Deformation and Fracture Processes in OF and OFF Copper William H Bowyer October 2004 ISSN 1104-1374 ISRN SKI-R-05/1 8-SE SKi SKI Perspective Background and purpose of the project The integrity of the canister is an important factor for long-term safety of the repository for spent nuclear fuel. When the canister is placed in the repository hole it will be subjected to mechanical loads due to the hydrostatical pressure and the swelling pressure of the bentonite surrounding it. Copper is a soft material and will creep and lay down on the ductile iron insert due to the loads. The creep process will go on until the bentonite is fully saturated. During this time period the creep properties of the copper canister are very essential for the integrity of the copper shell. The copper material may creep but is not supposed to fracture. SKB has investigated the creep properties of the used copper material (Oxygen Free Copper with 40 - 60 ppm phosphorous, OFP material), by carrying out different research projects regarding creep. All the relevant work arising from the development programme concentrates on measurement of minimum creep rates and creep lives for Oxygen free copper (OF) and OF to which 50ppm phosphorus has been added (OFP) under conditions where test duration has not exceeded two years. This has required testing to be accelerated by using higher temperatures and/or higher stresses than would be expected in service. Extrapolation of test data over five orders of magnitude in time, coupled with reductions in temperature and stress, has been used to predict service behaviour.
    [Show full text]
  • 9. Microphysics of Mantle Rheology
    9. Microphysics of Mantle Rheology Ge 163 5/7/14 Outline • Introduction • Vacancies and crystal imperfections • Diffusion Creep • Dislocation creep • Deformation maps • Viscosity in the Deep Mantle • Visco-elastic relaxation and thickness of the lithosphere • Role of Water in influencing creep strength • Appendix A • Details of the theory of Diffusion creep Why does elastic thickness (h, Te) increases with age ? Watts [2001] Diffusion Creep Diffusion creep is the migration or diffusion of point defects through the crystal lattice. An example of a point defect is a vacancy, where an atom is missing from the normal highly regular crystal lattice. Another is an impurity, where some species (of a minor concentration) exists or is located within the regular lattice. So the diffusion of a minor species becomes: b 2 1/2 φo ⎛ φo ⎞ −2φo /kT D = 2 ⎜ ⎟ e 3π kT ⎝ m ⎠ In general, the diffusion coefficient is a function of both temeprature and pressure and is expressed in the form: ⎛ E + pV ⎞ D = D exp − a a o ⎝⎜ RT ⎠⎟ where R is the gas constant, Ea is the activation energy, and Va is the activation volume. The pVa term takes into account of the effect of pressure in reducing the number of vacanies and increasing the potential energy barrier between lattice sites. Diffusion of atoms in a crystal in the presence of differential stress can result in creep. compression Poirier [1991] 12V D ε = a σ xx RTh2 This is "Diffusion Creep" (also known as Nabarro-Herring creep) which resuslts in a linear relation between strain-rate and stress. Recall that we have previously described a "constitutive relation" for a fluid as: σ = 2ηεxx ∴ the "viscosity" for a crystalline solid is: RTh2 η = 24VaD But substituting the relation that we have already derived for the D, the Diffusion 2 RTh ⎛ Ea + pVa ⎞ η = exp⎜ ⎟ 24VaDo ⎝ RT ⎠ In Nabarro-Herring creep, the atoms and vacanies diffuse through the interior of mineral grains.
    [Show full text]